Abstract

SUMMARY A Triangular Spectral Element Method (TSEM) is presented to simulate elastic wave propagation using an unstructured triangulation of the physical domain. TSEM makes use of a variational formulation of elastodynamics based on unstructured straight-sided triangles that allow enhanced flexibility when dealing with complex geometries and velocity structures. The displacement field is expanded into a high-order polynomial spectral approximation over each triangular subdomain. Continuity between the subdomains of the triangulation is enforced using a multidimensional Lagrangian interpolation built on a set of Fekete points of the triangle. High-order accuracy is achieved by resorting to an analytical computation of the associated internal product and bilinear forms leading to a non-diagonal mass matrix formulation. Therefore, the time stepping involves the solution of a sparse linear algebraic system even in the explicit case. In this paper the accuracy and the geometrical flexibility of the TSEM is explored. Comparison with classical spectral elements on quadrangular grids shows similar results in terms of accuracy and stability even for long simulations. Surface and interface waves are shown to be accurately modelled even in the case of complex topography with the TSEM. Numerical results are presented for 2-D canonical examples as well as more specific problems, such as 2-D elastic wave scattering by a cylinder embedded in an homogeneous half-space. They all illustrate the enhanced geometrical flexibility of the TSEM. This clearly suggests the need of further investigations in computational seismology specifically targeted towards efficient implementations of the TSEM both in the time and the frequency domain.

Highlights

  • Many problems in geophysics need to infer the physical and chemical parameter distributions of the Earth’s interior from information provided by seismic wave propagation through complex media

  • By means of piecewise continuous geometrical maps, spectral elements have higher geometrical flexibility than spectral or pseudo-spectral methods, which are mainly confined to smooth problems defined on simple domains that can be mapped onto the nd-cube, while retaining the spatial exponential convergence for locally smooth solutions with quasi-optimal dispersion errors

  • A Triangular Spectral Element Method (TSEM) is investigated within the context of elastic wave propagation in complex geological media

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Summary

INTRODUCTION

Many problems in geophysics need to infer the physical and chemical parameter distributions of the Earth’s interior from information provided by seismic wave propagation through complex media. We explore the use of the unstructured triangle based SEM introduced in Taylor & Wingate (2000) and Warburton et al (2000), relying on the use of the Dubiner’s polynomials (Koorwinder 1975; Dubiner 1991) and multivariate Lagrangian interpolation based on Fekete points (Taylor & Wingate 2000; Hesthaven & Teng 2000), for 2-D seismological applications in time domain with special attention to dispersion errors It is worth mentioning similar type of studies that have been recently conducted independently by Pasquetti & Rapetti (2004) in the context of Helmholtz equations, and Giraldo & Warburton (2005) in geophysical fluid dynamics. The paper ends up with a discussion of further research directions

THE ELASTODYNAMIC PROBLEM
Geometrical discretization
Piecewise polynomial approximation
Spectral expansion
Lagrangian interpolation
Interpolation points and inner products
Spectral element discretization
Time discretization
Bi-periodic elastic wave propagation in an homogeneous medium
Unstructured triangulation
The Lamb’s problem
The elastic wedge problem
75 Receivers51
Elastic scattering by a cylinder in a homogeneous half-space
Elastic half-space with free-surface and interface topographies
Findings
CONCLUSIONS
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